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NOAA's Rapid Response to the Howard A. Hanson Dam Flood Risk Management Crisis

Allen B. WhiteNOAA/Earth System Research Laboratory/Physical Sciences Division, Boulder, Colorado

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Brad ColmanNOAA/National Weather Service/WFO Seattle, Seattle, Washington

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Gary M. CarterNOAA/National Weather Service/Office of Hydrologic Development, Silver Spring, Maryland

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F. Martin RalphNOAA/Earth System Research Laboratory/Physical Sciences Division, Boulder, Colorado

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Robert S. WebbNOAA/Earth System Research Laboratory/Physical Sciences Division, Boulder, Colorado

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David G. BrandonNOAA/National Weather Service/Western Region Hydrology and Climate Services, Salt Lake City, Utah

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Clark W. KingNOAA/Earth System Research Laboratory/Physical Sciences Division, Boulder, Colorado

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Paul J. NeimanNOAA/Earth System Research Laboratory/Physical Sciences Division, Boulder, Colorado

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Daniel J. GottasNOAA/Earth System Research Laboratory/Physical Sciences Division, Boulder, Colorado

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Isidora JankovCooperative Institute for Research in the Atmosphere, Colorado State University, Fort Collins, and NOAA/Earth System Research Laboratory/Global Systems Division, Boulder, Colorado

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Keith F. BrillNOAA/National Weather Service/Hydrometeorological Prediction Center, Suitland, Maryland

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Yuejian ZhuNOAA/NWS/National Centers for Environmental Prediction/Environmental Modeling Center, Camp Springs, Maryland

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Kirby CookNOAA/National Weather Service/WFO Seattle, Seattle, Washington

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Henry E. BuehnerNOAA/National Weather Service/WFO Seattle, Seattle, Washington

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Harold OpitzNOAA/National Weather Service/Pacific Northwest RFC, Portland, Oregon

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David W. ReynoldsNOAA/National Weather Service/WFO San Francisco Bay Area, Monterey, California

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Lawrence J. SchickU.S. Army Corps of Engineers, Seattle, Washington

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The Howard A. Hanson Dam (HHD) has brought flood protection to Washington's Green River Valley for more than 40 years and opened the way for increased valley development near Seattle. However, following a record high level of water behind the dam in January 2009 and the discovery of elevated seepage through the dam's abutment, the U.S. Army Corps of Engineers declared the dam “unsafe.” NOAA's Office of Oceanic and Atmospheric Research (OAR) and National Weather Service (NWS) worked together to respond rapidly to this crisis for the 2009/10 winter season, drawing from innovations developed in NWS offices and in NOAA's Hydrometeorology Test-bed (HMT).

New data telemetry was added to 14 existing surface rain gauges, allowing the gauge data to be ingested into the NWS rainfall database. The NWS Seattle Weather Forecast Office produced customized daily forecasts, including longer-lead-time hydrologic outlooks and new decision support services tailored for emergency managers and the public, new capabilities enabled by specialized products from NOAA's National Centers for Environmental Prediction (NCEP) and from HMT. The NOAA Physical Sciences Division (PSD) deployed a group of specialized instruments on the Washington coast and near the HHD that constituted two atmospheric river (AR) observatories (AROs) and conducted special HMT numerical model forecast runs. Atmospheric rivers are narrow corridors of enhanced water vapor transport in extratropical oceanic storms that can produce heavy orographic precipitation and anomalously high snow levels, and thus can trigger flooding. The AROs gave forecasters detailed vertical profile observations of AR conditions aloft, including monitoring of real-time water vapor transport and comparison with model runs.

The Howard A. Hanson Dam (HHD) has brought flood protection to Washington's Green River Valley for more than 40 years and opened the way for increased valley development near Seattle. However, following a record high level of water behind the dam in January 2009 and the discovery of elevated seepage through the dam's abutment, the U.S. Army Corps of Engineers declared the dam “unsafe.” NOAA's Office of Oceanic and Atmospheric Research (OAR) and National Weather Service (NWS) worked together to respond rapidly to this crisis for the 2009/10 winter season, drawing from innovations developed in NWS offices and in NOAA's Hydrometeorology Test-bed (HMT).

New data telemetry was added to 14 existing surface rain gauges, allowing the gauge data to be ingested into the NWS rainfall database. The NWS Seattle Weather Forecast Office produced customized daily forecasts, including longer-lead-time hydrologic outlooks and new decision support services tailored for emergency managers and the public, new capabilities enabled by specialized products from NOAA's National Centers for Environmental Prediction (NCEP) and from HMT. The NOAA Physical Sciences Division (PSD) deployed a group of specialized instruments on the Washington coast and near the HHD that constituted two atmospheric river (AR) observatories (AROs) and conducted special HMT numerical model forecast runs. Atmospheric rivers are narrow corridors of enhanced water vapor transport in extratropical oceanic storms that can produce heavy orographic precipitation and anomalously high snow levels, and thus can trigger flooding. The AROs gave forecasters detailed vertical profile observations of AR conditions aloft, including monitoring of real-time water vapor transport and comparison with model runs.

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